Effects of stand density on soil respiration and labile organic carbon in different aged Larix principis-rupprechtii plantations

Ecological Processes

Daoli Peng¹  Tairui Liu¹  Yunxiang Zhang²  Jinping Guo²  Zhijie Tan³ 

[1] College of Forestry, Beijing Forestry University, No. 35 Tsinghua East Road, Haidian District, 100083, Beijing, People’s Republic of China;College of Forestry, Shanxi Agricultural University, 030801, Jingzhong, People’s Republic of China;Lvliang Bureau of Planning and Natural Resources, 033000, Lüliang, People’s Republic of China;

关键词: Stand density;    Soil respiration;    Soil organic carbon;    Soil labile organic carbon;    Influence mechanism;   

DOI  :  10.1186/s13717-021-00301-9

来源: Springer

【 摘 要 】

BackgroundThe carbon pools of forest soils play a vital role in global carbon sequestration and emissions. Forest management can regulate the sequestration and output of forest soil carbon pools to a certain extent; however, the kinetics of the effects of forest density on soil carbon pools require further investigation.MethodsWe established sample plots with stand density gradients in three different aged Larix principis-rupprechtii plantations and quantified the soil respiration, soil organic carbon (SOC), soil dissolved organic carbon (DOC), microbial biomass carbon (MBC), light fraction organic carbon (LFOC), and readily oxidized carbon (ROC).Results and conclusionsDuring the growth and development of plantations, stand density is an essential factor that impacts soil respiration and its associated elements. Moderate density was observed to promote both the soil and heterotrophic respiration rates and the sequestration of MBC and LFOC, whereas it inhibited the sequestration of ROC. The soil, heterotrophic, and autotrophic respiration rates of older forest stands were relatively rapid, whereas the contents of SOC, MBC, LFOC, DOC, and ROC were higher and more sensitive to changes in stand density. The MBC, LFOC, and ROC in soil labile organic carbon were closely related to both the soil and heterotrophic respiration, but not the SOC. Among them, the LFOC and MBC played the roles of “warehouse” and “tool” and were significantly correlated with soil and heterotrophic respiration. The ROC, as a “raw material”, exhibited a significantly negative correlation with the soil and heterotrophic respiration. When the soil and heterotrophic respiration rates were rapid, the ROC content in the soil maintained the low level of a “dynamically stabilized” state. The stand density regulated heterotrophic respiration by affecting the soil labile organic carbon, which provided an essential path for the stand density to regulate soil respiration.

【 授权许可】

CC BY